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Climatic Regions Of India
The climate of India consists of a wide range of weather conditions across a vast geographic scale and varied topography. Based on the Köppen system, India hosts six major climatic sub types, ranging from arid deserts in the west, alpine tundra and glaciers in the north, and humid tropical regions supporting rain forests in the southwest and the island territories. Many regions have starkly different microclimates, making it one of the most climatically diverse countries in the world. The country's meteorological department follows the international standard of four seasons with some local adjustments: winter (December to February), summer (March to May), monsoon (rainy) season (June to September), and a post-monsoon period (October and November). India's geography and geology are climatically pivotal: the Thar Desert in the northwest and the Himalayas in the north work in tandem to create a culturally and economically important monsoonal regime. As Earth's highest and most ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Valley Of Flowers Uttaranchal Full View
A valley is an elongated low area often running between Hill, hills or Mountain, mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacier, glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glaciation, glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In karst, areas of limestone bedrock, dry valleys may also result from drainage now taking place cave, underground rather than at the surface. Rift valleys arise principally from tectonics, earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tropic Of Cancer
The Tropic of Cancer, which is also referred to as the Northern Tropic, is the most northerly circle of latitude on Earth at which the Sun can be directly overhead. This occurs on the June solstice, when the Northern Hemisphere is tilted toward the Sun to its maximum extent. It also reaches 90 degrees below the horizon at solar midnight on the December Solstice. Using a continuously updated formula, the circle is currently north of the Equator. Its Southern Hemisphere counterpart, marking the most southerly position at which the Sun can be directly overhead, is the Tropic of Capricorn. These tropics are two of the five major circles of latitude that mark maps of Earth, the others being the Arctic and Antarctic circles and the Equator. The positions of these two circles of latitude (relative to the Equator) are dictated by the tilt of Earth's axis of rotation relative to the plane of its orbit, and since the tilt changes, the location of these two circles also changes. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Supercontinent
In geology, a supercontinent is the assembly of most or all of Earth's continent, continental blocks or cratons to form a single large landmass. However, some geologists use a different definition, "a grouping of formerly dispersed continents", which leaves room for interpretation and is easier to apply to Precambrian times. To separate supercontinents from other groupings, a limit has been proposed in which a continent must include at least about 75% of the continental crust then in existence in order to qualify as a supercontinent. Supercontinents have assembled and dispersed multiple times in the geologic past (see table). According to modern definitions, a supercontinent does not exist today; the closest in existence to a supercontinent is the current Afro-Eurasian landmass, which covers approx. 57% of Earth's total land area. The last time the continental landmasses were near to one another was 336 to 175 million years ago as the supercontinent, Pangaea. The positions of con ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Year
A year or annus is the orbital period of a planetary body, for example, the Earth, moving in its orbit around the Sun. Due to the Earth's axial tilt, the course of a year sees the passing of the seasons, marked by change in weather, the hours of daylight, and, consequently, vegetation and soil fertility. In temperate and subpolar regions around the planet, four seasons are generally recognized: spring, summer, autumn and winter. In tropical and subtropical regions, several geographical sectors do not present defined seasons; but in the seasonal tropics, the annual wet and dry seasons are recognized and tracked. A calendar year is an approximation of the number of days of the Earth's orbital period, as counted in a given calendar. The Gregorian calendar, or modern calendar, presents its calendar year to be either a common year of 365 days or a leap year of 366 days, as do the Julian calendars. For the Gregorian calendar, the average length of the calendar year (t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Triassic
The Triassic ( ) is a geologic period and system which spans 50.6 million years from the end of the Permian Period 251.902 million years ago ( Mya), to the beginning of the Jurassic Period 201.36 Mya. The Triassic is the first and shortest period of the Mesozoic Era. Both the start and end of the period are marked by major extinction events. The Triassic Period is subdivided into three epochs: Early Triassic, Middle Triassic and Late Triassic. The Triassic began in the wake of the Permian–Triassic extinction event, which left the Earth's biosphere impoverished; it was well into the middle of the Triassic before life recovered its former diversity. Three categories of organisms can be distinguished in the Triassic record: survivors from the extinction event, new groups that flourished briefly, and other new groups that went on to dominate the Mesozoic Era. Reptiles, especially archosaurs, were the chief terrestrial vertebrates during this time. A specialized subgroup of archo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nainital Snow Lake
Nainital ( Kumaoni: ''Naintāl''; ) is a city and headquarters of Nainital district of Kumaon division, Uttarakhand, India. It is the judicial capital of Uttarakhand, the High Court of the state being located there and is the headquarters of an eponymous district. It also houses the Governor of Uttarakhand, who resides in the Raj Bhavan. Nainital was the summer capital of the United Provinces. Nainital is located in the Kumaon foothills of the Jagbeer Himalayas at a distance of from the state capital Dehradun and from New Delhi, the capital of India. Situated at an altitude of above sea level, the city is set in a valley containing an eye-shaped lake, approximately two miles in circumference, and surrounded by mountains, of which the highest are Naina Peak () on the north, Deopatha () on the west, and Ayarpatha () on the south. From the tops of the higher peaks, "magnificent views can be obtained of the vast plain to the south, or of the mass of tangled ridges lying no ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gurudongmar North Sikkim Himalayas India
Gurudongmar Lake is one of the highest lakes in the world and in India, at an elevation of according to the Government of Sikkim. It is located in the Great Himalayas in the Mangan District in Indian state of Sikkim, and considered sacred by Buddhists, Sikhs and Hindus. The lake is named after Guru Padmasambhava—also known as Guru Rinpoche—founder of Tibetan Buddhism, who visited in the 8th century. Geography The high altitude lake is located away from Gangtok, the capital city of Sikkim, and about south of the Tibetan (Chinese) border, in the district of North Sikkim. The lake can be reached by road from Lachen via Thangu Valley. The road from Thangu to Gurudongmar passes through rugged terrain with moraine, which has high alpine pastures covered with many rhododendron trees. While Indian tourists are allowed to visit the lake, foreigners need to get a special permit from the Ministry of Home Affairs in Delhi. Features The lake, fed by glaciers, is located to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ladakh India Monsoon Clouds
Ladakh () is a region administered by India as a union territory which constitutes a part of the larger Kashmir region and has been the subject of dispute between India, Pakistan, and China since 1947. (subscription required) Quote: "Jammu and Kashmir, state of India, located in the northern part of the Indian subcontinent in the vicinity of the Karakoram and westernmost Himalayan mountain ranges. From 1947 to 2019, Ladakh was part of the Indian state of Jammu and Kashmir, which has been the subject of dispute between India, Pakistan, and China since the partition of the subcontinent in 1947." Quote: "Jammu and Kashmir: Territory in northwestern India, subject to a dispute between India and Pakistan. It has borders with Pakistan and China." Ladakh is bordered by the Tibet Autonomous Region to the east, the Indian state of Himachal Pradesh to the south, both the Indian-administered union territory of Jammu and Kashmir and the Pakistan-administered Gilgit-Baltistan to the wes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cherrapunji
Cherrapunji () or Sohra is a subdivisional town (Proposed District) East Khasi Hills district in the Indian state of Meghalaya. It is the traditional capital of ka ''hima'' Sohra (Khasi tribal kingdom). Sohra has often been credited as being the wettest place on Earth, but for now nearby Mawsynram currently holds that distinction. It still holds the all-time record for the most rainfall in a calendar month and in a year, however: it received in July 1861 and between 1 August 1860 and 31 July 1861. History The history of the Khasi people – native inhabitants of Sohra– may be traced from the early part of the 16th century. Between the 16th and 18th centuries, these people were ruled by their tribal 'Syiems (rajas or chiefs) of Khyriem' in the Khasi Hills. The Khasi hills came under British authority in 1833 with the submission of the last of the important Syiem, Tirot Sing Syiem. The main pivot on which the entire superstructure of Khasi society rests is the matrilineal ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kalinagar Floods B
Kalinagar is a town and a nagar panchayat in Pilibhit district in the Indian state of Uttar Pradesh. Kalinagar is a new tehsil of district Pilibhit Pin code -262124 Geography Kalinagar is located at . It has an average elevation of 184 metres (603 feet). Demographics As of the 2001 Census of India The 2001 Census of India was the 14th in a series of censuses held in India every decade since 1871. The population of India was counted as 1,028,737,436 consisting of 532,223,090 males and 496,514,346 females. Total population increased by 18 ..., Kalinagar had a population of 9,984. Males constitute 53% of the population and females 47%. Kalinagar has an average literacy rate of 34%, lower than the national average of 59.5%: male literacy is 45%, and female literacy is 22%. In Kalinagar, 20% of the population is under 6 years of age. References Cities and towns in Pilibhit district {{Pilibhit-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
